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To begin the analysis, a part of fault tree has been drawn in Figure 1.
Shallow seismicity is relatively low in the middle part of fault.
Creep movement has reported from the electro-optical distance measurements at the central part of fault (Geographical Survey Institute, 2000).
In 4.3 we interpreted that extensional stress is relatively larger in the central part of fault than in the southwestern edge.
In addition to many strike-slip type focal mechanisms in the Atotsugawa area, some events particularly in the southwestern part of fault exhibit dip-slip mechanisms having inconsistent P-axes with the fault movement.
Since the seismicity in Fig. 3 is quite similar to that by Mikumo et al. (1988) in a period from 1980 to 1986, it is clear that there was a temporal change in seismicity in the central part of fault.
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The results of this paper can be utilized in several ways, as stand-alone fault-tolerant state estimation techniques, as an essential part of fault-tolerant state feedback controller design, as fault-sensitive filters or as a bank of filters for multiple model fault detection and isolation schemes.
Fault zone permeability for parts of fault 1 is <1 mD while parts of faults 2 and 3 are >1 mD.
We will consider two parts of fault detection systems by using the information of PDF in the following section.
It is found by comparing development well productivity of parts of Fault F234 with different strikes that the development wells at edge of NNW-striking faults have higher productivity (Fig. 3) and richer remaining oil.
Fault latency is part of the fault model.
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